Extremely H<sub>2</sub>-Rich Fluid Inclusions in Eclogite from Dabie Shan Orogenic Belt, Eastern China

Authors

  • Xiao-Yong
     School of Earth and Space Sciences, University of Science and Technology of China, Hefei - 230 026
  • De-Lian Liu
     School of Earth and Space Sciences, University of Science and Technology of China, Hefei - 230 026
  • Jin-Xing Dai
     School of Earth and Space Sciences, University of Science and Technology of China, Hefei - 230 026

Abstract

The eclogites Sra the Dabie Shan terranes have recorded the phpsico-chemical properties of cmstal materials which underwent the Triassic ultra-high pressure (UHF) metamorphism at mantle depths. Identification of coesite and micro-diamond in different eclogite localities of the region (Okay et al. 1989; Wang et a1. 1989; Xu et A. 1992) demonstrates, that supracrustal materials can be subducted to mantle depth of at least 120 km. This paper reports extremely rich H2-bearing fluid inclusions from UHP edogites from the Dabie Shan orogenic belt,

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Issue

Volume 61, Issue 1, January 2003

Section

Short Communications

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Published

2003-01-01

How to Cite

Xiao-Yong, ., Liu, D.-L., & Dai, J.-X. (2003). Extremely H<sub>2</sub>-Rich Fluid Inclusions in Eclogite from Dabie Shan Orogenic Belt, Eastern China. Journal of Geological Society of India, 61(1), 101–102. Retrieved from https://www.geosocindia.com/index.php/jgsi/article/view/83461